Oligocene molluscan biostratigraphy and paleontology of the lower part of the type Temblor Formation, California: Marine mollusks from the basal shale (Cymric Shale Member) and the overlying sandstone (Wygal Sandstone Member) are of provincial Oligocene age. Warm-water assemblages from the Wygal Sandstone Member represent a previously unrecognized biostratigraphic unit of late Oligocene age in California
Gespeichert in:
| 1. Verfasser: | |
|---|---|
| Format: | Buch |
| Sprache: | English |
| Veröffentlicht: |
Washington
U.S. Gov. Print. Off.
1973
|
| Schriftenreihe: | Geological Survey professional paper
791 |
| Beschreibung: | IV, 48 S., [9] Bl. Ill., Kt. |
Internformat
MARC
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| 100 | 1 | |a Addicott, Warren O. |e Verfasser |4 aut | |
| 245 | 1 | 0 | |a Oligocene molluscan biostratigraphy and paleontology of the lower part of the type Temblor Formation, California |b Marine mollusks from the basal shale (Cymric Shale Member) and the overlying sandstone (Wygal Sandstone Member) are of provincial Oligocene age. Warm-water assemblages from the Wygal Sandstone Member represent a previously unrecognized biostratigraphic unit of late Oligocene age in California |c by Warren O. Addicott |
| 264 | 1 | |a Washington |b U.S. Gov. Print. Off. |c 1973 | |
| 300 | |a IV, 48 S., [9] Bl. |b Ill., Kt. | ||
| 336 | |b txt |2 rdacontent | ||
| 337 | |b n |2 rdamedia | ||
| 338 | |b nc |2 rdacarrier | ||
| 490 | 1 | |a Geological Survey professional paper |v 791 | |
| 830 | 0 | |a Geological Survey professional paper |v 791 |w (DE-604)BV000005472 |9 791 | |
| 999 | |a oai:aleph.bib-bvb.de:BVB01-027276338 | ||
Datensatz im Suchindex
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| any_adam_object | |
| author | Addicott, Warren O. |
| author_facet | Addicott, Warren O. |
| author_role | aut |
| author_sort | Addicott, Warren O. |
| author_variant | w o a wo woa |
| building | Verbundindex |
| bvnumber | BV041831451 |
| ctrlnum | (OCoLC)879961719 (DE-599)BSZ075777487 |
| dewey-full | 564 |
| dewey-hundreds | 500 - Natural sciences and mathematics |
| dewey-ones | 564 - Fossil Mollucas & Molluscoidea |
| dewey-raw | 564 |
| dewey-search | 564 |
| dewey-sort | 3564 |
| dewey-tens | 560 - Paleontology |
| discipline | Geologie / Paläontologie |
| format | Book |
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| id | DE-604.BV041831451 |
| illustrated | Illustrated |
| indexdate | 2024-07-10T01:06:25Z |
| institution | BVB |
| language | English |
| oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-027276338 |
| oclc_num | 879961719 |
| open_access_boolean | |
| owner | DE-19 DE-BY-UBM |
| owner_facet | DE-19 DE-BY-UBM |
| physical | IV, 48 S., [9] Bl. Ill., Kt. |
| publishDate | 1973 |
| publishDateSearch | 1973 |
| publishDateSort | 1973 |
| publisher | U.S. Gov. Print. Off. |
| record_format | marc |
| series | Geological Survey professional paper |
| series2 | Geological Survey professional paper |
| spelling | Addicott, Warren O. Verfasser aut Oligocene molluscan biostratigraphy and paleontology of the lower part of the type Temblor Formation, California Marine mollusks from the basal shale (Cymric Shale Member) and the overlying sandstone (Wygal Sandstone Member) are of provincial Oligocene age. Warm-water assemblages from the Wygal Sandstone Member represent a previously unrecognized biostratigraphic unit of late Oligocene age in California by Warren O. Addicott Washington U.S. Gov. Print. Off. 1973 IV, 48 S., [9] Bl. Ill., Kt. txt rdacontent n rdamedia nc rdacarrier Geological Survey professional paper 791 Geological Survey professional paper 791 (DE-604)BV000005472 791 |
| spellingShingle | Addicott, Warren O. Oligocene molluscan biostratigraphy and paleontology of the lower part of the type Temblor Formation, California Marine mollusks from the basal shale (Cymric Shale Member) and the overlying sandstone (Wygal Sandstone Member) are of provincial Oligocene age. Warm-water assemblages from the Wygal Sandstone Member represent a previously unrecognized biostratigraphic unit of late Oligocene age in California Geological Survey professional paper |
| title | Oligocene molluscan biostratigraphy and paleontology of the lower part of the type Temblor Formation, California Marine mollusks from the basal shale (Cymric Shale Member) and the overlying sandstone (Wygal Sandstone Member) are of provincial Oligocene age. Warm-water assemblages from the Wygal Sandstone Member represent a previously unrecognized biostratigraphic unit of late Oligocene age in California |
| title_auth | Oligocene molluscan biostratigraphy and paleontology of the lower part of the type Temblor Formation, California Marine mollusks from the basal shale (Cymric Shale Member) and the overlying sandstone (Wygal Sandstone Member) are of provincial Oligocene age. Warm-water assemblages from the Wygal Sandstone Member represent a previously unrecognized biostratigraphic unit of late Oligocene age in California |
| title_exact_search | Oligocene molluscan biostratigraphy and paleontology of the lower part of the type Temblor Formation, California Marine mollusks from the basal shale (Cymric Shale Member) and the overlying sandstone (Wygal Sandstone Member) are of provincial Oligocene age. Warm-water assemblages from the Wygal Sandstone Member represent a previously unrecognized biostratigraphic unit of late Oligocene age in California |
| title_full | Oligocene molluscan biostratigraphy and paleontology of the lower part of the type Temblor Formation, California Marine mollusks from the basal shale (Cymric Shale Member) and the overlying sandstone (Wygal Sandstone Member) are of provincial Oligocene age. Warm-water assemblages from the Wygal Sandstone Member represent a previously unrecognized biostratigraphic unit of late Oligocene age in California by Warren O. Addicott |
| title_fullStr | Oligocene molluscan biostratigraphy and paleontology of the lower part of the type Temblor Formation, California Marine mollusks from the basal shale (Cymric Shale Member) and the overlying sandstone (Wygal Sandstone Member) are of provincial Oligocene age. Warm-water assemblages from the Wygal Sandstone Member represent a previously unrecognized biostratigraphic unit of late Oligocene age in California by Warren O. Addicott |
| title_full_unstemmed | Oligocene molluscan biostratigraphy and paleontology of the lower part of the type Temblor Formation, California Marine mollusks from the basal shale (Cymric Shale Member) and the overlying sandstone (Wygal Sandstone Member) are of provincial Oligocene age. Warm-water assemblages from the Wygal Sandstone Member represent a previously unrecognized biostratigraphic unit of late Oligocene age in California by Warren O. Addicott |
| title_short | Oligocene molluscan biostratigraphy and paleontology of the lower part of the type Temblor Formation, California |
| title_sort | oligocene molluscan biostratigraphy and paleontology of the lower part of the type temblor formation california marine mollusks from the basal shale cymric shale member and the overlying sandstone wygal sandstone member are of provincial oligocene age warm water assemblages from the wygal sandstone member represent a previously unrecognized biostratigraphic unit of late oligocene age in california |
| title_sub | Marine mollusks from the basal shale (Cymric Shale Member) and the overlying sandstone (Wygal Sandstone Member) are of provincial Oligocene age. Warm-water assemblages from the Wygal Sandstone Member represent a previously unrecognized biostratigraphic unit of late Oligocene age in California |
| volume_link | (DE-604)BV000005472 |
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